|
|
Norsk versjon | ||||
| THE ORE DATABASE | |||||
| Deposit Area 1653 - 015 | |||||
| (Last updated 27.jan.2023) | |||||
Name of Deposit Area : Havdal |
| (Object Id : 1653,015,00,00) |
| Location |
| County : | Sør-Trøndelag (16) | Municipality : | Melhus (1653) |
| Map 1:50000: | Trondheim (1621-4) | Map 1:250000: | Trondheim |
| Marking point: | Longitude: | 10.3640060 | Latitude: | 63.2972960 |
| EU89-UTM Zone 32 | (Coordinates IS confirmed) |
| X-coord: | 568382 m. | Y-coord: | 7019440 m. |
|
|
| Commodity |
| Main Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Sub Type: | Sulphides | |
| Element(s): | Kis |
| Production |
| Activity: | Pitting | Reserves: | ||
| Prod. method: | Production: | |||
| Prod. status: | Volume of dump: | 20 m3 |
| Importance |
| Public: | Not Assessed (reg. 18.02.2015) |
| Economical: | Minor interest , (Confirmed 05.nov.2021 by Jan Sverre Sandstad) |
Operations |
| From - To | Activity | Comments | |
| 2021 - 2021 | Sampling | Company/Institution :NGU |
Mineralization |
| Era: | Paleozoic | Period: | Ordovician | |
| Dating: | Method: | |||
| Genesis: | Volcex | Form: | Irregular | |
| Main texture: | Structureless | Min. distribution: | Disseminated (<20 % ore minerals) |
| Main grain size: | Fine grained (< 1 mm) | Main alteration: | Chloritisation |
| Strike/Dip: | Direction: | |||
| Plunge: |
| Stratigraphic classification of host rock |
| Era: | Paleozoic | Period: | Ordovician |
| Province: | Caledonides | |
| Geotec.unit: | Trondheim Nappe Complex | |
| Tectonic complex: | LVB ofiolittfragmenter | |
| Igneous complex: |
| Group: | Formation: | Bymarkgrønnsteinen |
Mineralogy |
| Relationship | Mineral | Amount | |
| Gangue mineral | Amphibole | Major mineral (>10%) | |
| Gangue mineral | Feldspar | Major mineral (>10%) | |
| Gangue mineral | Chlorite | Subordinate mineral (1-10%) | |
| Gangue mineral | Quartz | Subordinate mineral (1-10%) | |
| Ore mineral | Pyrite | Major mineral (>10%) |
Lithology: |
| Relationship | Rock | Origin | |
| Host rock | Greenstone | Extrusive Original rock :Basalt |
|
| Metamorphic facies :Greenschist |
Structures |
| Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
| Host rock | Schistosity | Strike/Dip :30 / 25 | Post-mineralisation |
Information(s) in free text format |
| Free text |
| Forekomsten ligger ved en tursti som kan følges opp sørover fra gården Havdal. Det består av en 10-12 m lang dagskjæring langs nordsida av en NØ-SV orientert skrent som er opptil 3 m høy. Skrenten består av sterkt rustfarget, flattliggende grønnstein med tynne sulfidførende årer og svak disseminasjon av svovelkis. Tippen er svært overgrodd og mer massiv sulfidmineralisering ble ikke påvist. |
Fieldsamples |
| Sample No. | Sample type | Miscellanrous | ||||
| JS-T2109 | Dump |
|
| NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
| from |
| Deposit Area 1653 - 015 Havdal |
Element analyses |
( *=parts pr. million, #=parts pr.billion, Negative values means below detection limit value.) |
| Sample No. | Sample Type | Cu* | Zn* | Pb* | Co* | Ni* | Ag* | Au# |
| JS-T2109 | Dump | 2580 | 495 | 13 | 49 | 3 | 1.5 | 3.0 |
| ------------------ |
| Sample No. | Pt# | Pd# | As* | Cd* | Ba* | Mo* | Sn* | Sb* | Bi* |
| JS-T2109 | -5.0 | -1.0 | 6 | .9 | -10 | 4.12 | 1 | -0 | 0 |
| ------------------ |
| Sample No. | Se* | Ga* | Ge* | In* | S% | V* | Cr* | Mn* | Fe% |
| JS-T2109 | 6.00 | 18.45 | 0.13 | 0.39 | 5.20 | 325 | -1 | 3350 | 13.95 |
| ------------------ |
| Sample No. | Th* | U* | W* | Rb* | Sr* | Y* | Zr* | Nb* | Ta* |
| JS-T2109 | 0.69 | 0.10 | 0 | 0.1 | 13.5 | 38.0 | 62 | 2.10 | 0.15 |
| ------------------ |
| Sample No. | Cs* | La* | Ce* | Li* | Be* | P* | Sc* | Te* | Hf* |
| JS-T2109 | -0.05 | 5.50 | 15.80 | 11 | 0 | 770 | 26.50 | 0.13 | 2.40 |
| ------------------ |
| Sample No. | Re* | Tl* | |||||||
| JS-T2109 | 10 | -0 |
| The fact sheet was created on 19.05.2024 |
| Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
| Copyright © 2024 Geological Survey of Norway |